El Niño and La Niña sea surface temperature anomalies: Asymmetry characteristics associated with their wind stress anomalies

By I. Kang, J. Kug. 2002

206 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/8772dbd6921aaa1d018733d5bc13afe89a42594e

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Jochem Marotzke
2. Johann Jungclaus
3. T. Bayr
4. Claudia Frauen
5. D. Dommenget
6. Helmuth Haak
7. F. Jin
8. H. Ueda

In Global and Planetary Change

1. Jochem Marotzke
2. Johann Jungclaus
3. T. Bayr
4. Helmuth Haak
5. Claudia Frauen
6. D. Dommenget
7. F. Jin
8. H. Ueda

In Oceanography

1. Jochem Marotzke
2. T. Bayr
3. Johann Jungclaus
4. Claudia Frauen
5. D. Dommenget
6. Helmuth Haak
7. H. Ueda
8. M. Ohba

Citations in the corpus

• The unique 2009–2010 El Niño event: A fast phase transition of warm pool El Niño to La Niña (2011, background): “The westerly anomaly is confined to the west of dateline during its developing phase like other WP cases (Figure 4b), but expands to the central Pacific during its mature phase where the wind stress forcing is more effective in producing oceanic disturbances [Kang and Kug, 2002].”
• Characteristics of the ocean simulations in the Max Planck Institute Ocean Model (MPIOM) the ocean component of the MPI‐Earth system model (2013, background): “Determining the reason for this behavior is beyond the scope of this paper, but there are indications that this might be related to the modeled nonlinear response of the central Pacific zonal wind stress to SST anomalies [Kang and Kug, 2002; Frauen and Dommenget, 2010].”
• A Proposed Mechanism for the Asymmetric Duration of El Niño and La Niña (2011, background): “A proposed mechanism for the asymmetric duration of El Niño and La Niña”
• Combination Mode Dynamics of the Anomalous Northwest Pacific Anticyclone (2015, background): “First, La Niña events exhibit a weaker SST anomaly amplitude compared to El Niño events in nature (positive ENSO skewness) and hence generate a weaker anomalous circulation response (e.g., Kang and Kug 2002; Wu et al. 2010a; Stuecker et al. 2013).”
• Analysis of the non-linearity in the pattern and time evolution of El Niño southern oscillation (2013, background): “This basic structure of observed non-linearity in the zonal winds has also been described in Kang and Kug (2002) and Ohba and Ueda (2009). • As in the SST and SLP evolution we also find that the zonal wind anomalies prior to the peak of strong El Niño events are stronger (per NINO3.”
• Role of Nonlinear Atmospheric Response to SST on the Asymmetric Transition Process of ENSO (2009, methodology): “Our simple experiment is relatively similar to those in Kang and Kug (2002), but focuses on the self-transition process.”